云开地块晚二叠世富Fe-Ti-P超镁铁质岩的年代学、地球化学与岩石成因

周岱; 柯贤忠; 王祥东; 王磊; 王晶

doi:10.3799/dqkx.2020.275

Volume 46 Issue 4

Apr. 2021

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Zhou Dai, Ke Xianzhong, Wang Xiangdong, Wang Lei, Wang Jing, 2021. Geochronology, Geochemistry and Petrogenesis of Late Permian Fe-Ti-P-Rich Ultramafic Rocks in Yunkai Terrane, South China. Earth Science, 46(4): 1295-1310. doi: 10.3799/dqkx.2020.275

Citation:

Zhou Dai, Ke Xianzhong, Wang Xiangdong, Wang Lei, Wang Jing, 2021. Geochronology, Geochemistry and Petrogenesis of Late Permian Fe-Ti-P-Rich Ultramafic Rocks in Yunkai Terrane, South China. Earth Science, 46(4): 1295-1310. doi: 10.3799/dqkx.2020.275

Citation:

Zhou Dai, Ke Xianzhong, Wang Xiangdong, Wang Lei, Wang Jing, 2021. Geochronology, Geochemistry and Petrogenesis of Late Permian Fe-Ti-P-Rich Ultramafic Rocks in Yunkai Terrane, South China. Earth Science, 46(4): 1295-1310. doi: 10.3799/dqkx.2020.275

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Geochronology, Geochemistry and Petrogenesis of Late Permian Fe-Ti-P-Rich Ultramafic Rocks in Yunkai Terrane, South China

doi: 10.3799/dqkx.2020.275

Zhou Dai^{1, 2
,
,},
Ke Xianzhong^{1, 2},
Wang Xiangdong^{1, 2},
Wang Lei^{1, 2},
Wang Jing^{1, 2}

1.
Wuhan Center of Geological Survey, China Geological Survey, Wuhan 430205, China
2.
Research Center for Petrogenesis and Mineralization of Granitoid Rocks, Wuhan 430223, China

Received Date: 2020-06-15
Publish Date: 2021-04-15

Abstract

Abstract

In order to better understand the complex tectonic framework on the southern margin of South China block (SCB) between Permian and Triassic, the petrology, geochemistry and chronology of three newly discovered Late Permian ultramafic intrusions in the Yunkai area of West Guangdong were studied. These rocks are located at Yangchun Sanjia on the eastern edge of the Yunkai terrane and at Gaozhou Dajing and Dong'an in the middle of the Yunkai terrane. They are intrusive rocks in schist and paragneiss of the Yunkai Group and out putted as laccoliths or dykes which main lithologies are pyroxenite, hornblendite, amphibolite and plagioclase amphibolite. Zircon SHRIMP and LA-ICP-MS U-Pb age of ultramafic rocks are 253-259 Ma. These intrusive rocks are rich in titanomagnetite, titanite and apatite, showing strong enrichment of Fe-Ti-P, and exhibiting moderate enrichment of LREE and depletion in Nb-Ta-Zr-Hf. Ultramafic rocks exhibit relatively low ε_Nd(t)(-3.4 to -10.0) of whole rocks, ε_Hf(t) (-1.2 to -9.5) and δ¹⁸O(7.01‰-9.71‰) values of zircon, showing the enriched lithosphere mantle source affinity. In this study, it is suggested that the influence range of Permian Emeishan mantle plume(~259 Ma) may have spread to Yunkai area. Yunkai Late Permian ultramafic intrusions are generated from the partial melting of the lithospheric mantle which resulted from heat flow of mantle plume. Fe-Ti-P-rich minerals were assembled at the late stage of magma crystallization.
- Yunkai terrane,
- ultramafic,
- Emeishan mantle plume,
- zircon Hf-O isotope,
- geochemistry

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References(76)

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